|2009 Portland GSA Annual Meeting (18-21 October 2009)|
|Paper No. 159-5|
|Presentation Time: 9:00 AM-9:15 AM|
THE LATE ORDOVICIAN GLACIATION AND MASS EXTINCTION: RELATION TO BASALTIC WEATHERING AND VOLCANIC DEGASSING?
SALTZMAN, Matthew R., School of Earth Sciences, The Ohio State University, 275 Mendenhall Laboratory, 125 South Oval Mall, Columbus, OH 43210, firstname.lastname@example.org, YOUNG, Seth A., Department of Geological Sciences, Indiana University, 1001 E. 10th St, Bloomington, IN 47405, KUMP, Lee R., Department of Geosciences, Pennsylvania State University, University Park, PA 16802, FOLAND, Kenneth A., Department of Geological Sciences, The Ohio State Univ, 275 Mendenhall Laboratory, 125 South Oval Mall, Columbus, OH 43210, and LESLIE, Stephen A., Department of Geology and Environmental Sciences, James Madison University, MSC 6903, Harrisonburg, VA 22807|
The Late Ordovician mass extinction occurred during an enigmatic, short-lived (~ 106-107 yrs) glacial episode in a greenhouse world. We propose a link between global cooling during the Late Ordovician and relative rates of volcanic degassing and weathering. Evidence for volcanic (basaltic) weathering is based on the evidence for a large Ordovician drop in seawater 87Sr/86Sr (from ~ 0.709 to 0.708) that is among the most rapid in the entire Phanerozoic. 87Sr/86Sr measurements from eastern and western Laurentia indicate the rapid drop began in the P. serra conodont zone of the upper Darriwilian Stage (Middle Ordovician). The late Darriwilian is also a time of substantial volcanism as seen in the abundant deposition of altered volcanic ash deposits (K-bentonites).
We use a numerical model to explore the hypothesis that CO2 consumption during Middle to Late Ordovician volcanic weathering (which provided the flux of non-radiogenic Sr to the oceans) was closely balanced by volcanic outgassing. This produces steady pCO2 levels and climate through the middle Katian Stage of the Late Ordovician, consistent with recent Ordovician paleotemperature estimates based on conodont δ18O. In the late Katian, outgassing is reduced, consistent with the lack of K-bentonites in sedimentary successions, while volcanic weathering continues to draw down pCO2 and results in a cooling episode leading into the well known end-Ordovician (Hirnantian) glaciation.
2009 Portland GSA Annual Meeting (18-21 October 2009)
General Information for this Meeting
|Session No. 159|
Volcanism, Impacts, Mass Extinctions, and Global Environmental Change III
Oregon Convention Center: Portland Ballroom 253
8:00 AM-12:00 PM, Tuesday, 20 October 2009
Geological Society of America Abstracts with Programs, Vol. 41, No. 7, p. 418
© Copyright 2009 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.